The stochastic-conceptual rainfall-runoff simulator (SCRRS) developed by R.
A. Freeze in 1980 was used in this study to demonstrate quantitatively the
interplay of the factors that control the occurrence of overland flow by t
he Horton and Dunne mechanisms. The simulation domain and input data for th
e SCRRS simulations reported here were abstracted from the R-5 catchment (C
hickasha, OK) data sets. The results illustrate that the identification of
a dominant hydrological response process may not be as simple as a singular
Horton or Dunne characterization. The SCRRS simulations show that the Hort
on and Dunne processes can (i) occur simultaneously at different locations
during a given rainfall event, (ii) change from one process to the other wi
th time depending on the characteristics of the rainfall event, and (iii) b
e strongly dependent on the initial conditions. Copyright (C) 2001 John Wil
ey & Sons, Ltd.